New York City could face damaging floods ‘every five years’ in a warmer climate

FloodsNew York City could face damaging floods ‘every five years’ in a warmer climate

New York City could be struck by severe flooding up to every five years by 2030-45 if no efforts are made to curb human-driven climate change, new research finds.

Floods that reach more 2.25m in height – enough to inundate the first story of a building – could dramatically increase in frequency as a result of future sea level rise and bigger storm surges, the study suggests. Such severe floods would be expected only around once in every 25 years during 1970–2005.

The findings make it clear that “[flood] adaptation measures are critical to protect lives and infrastructure in a changing climate”, the lead author tells Carbon Brief.

Flooding threat

Like many coastal cities in the US, New York is vulnerable to flooding driven by storm surges from tropical cyclones, as well as sea level rise. In 2012, Hurricane Sandy overwhelmed the city with floodwater, killing 43 people and causing close to $50bn in damages.

Storm surges occur when a storm weather system moves from the sea to the land. As the weather system moves over the sea surface, its low pressure centre pulls up the surface of the water. Then, as the storm blows towards land, wind pushes the sea towards the coast, hitting the shore with large waves.

The height of these waves is dependent on the underlying sea level, the tide, and the size of the tropical cyclone. As sea levels rise, a storm surge has more chance of breaching coastal flood defences.

During Hurricane Sandy, the combined impact of the storm surge and a high tide saw sea levels reach a record height of 3.44m.

Storm surges

To understand how climate change could affect the future risk of coastal flooding in New York, researchers used models to simulate the behaviour of future tropical storms, as well as sea level rise in its surrounding waters.

Using a collection of global climate models,, the researchers gathered information about factors that impact the behaviour of a tropical storms. These factors include air temperature, humidity, sea surface temperature and wind speed.

“Using this information, we can generate a set of storms whose behaviour is consistent with a range of different climates. Each of these storms has their own unique set of characteristics, such as wind speed and pressure field.”

The researchers then used a storm surge model (known as ADCIRC) to generate the expected surge that each synthetic storm could create at The Battery, a public park located at the southern tip of Manhattan Island.

The results suggest that storms are likely to become larger and more powerful in the coming decades. (Carbon Brief has previously explored the link between climate change and tropical storms.)

However, a rise in storm intensity may not necessarily affect the size of storm surges, says Garner. This is because changes in ocean conditions in a warmer climate could cause tropical storms to shift eastwards, away from New York City. She says:

“As we move from the modern time period into the future, we find that storms tend to become more intense, while simultaneously shifting somewhat eastward, away from New York City. The increase in storm intensity is compensated by the shift in storm tracks. That is, changing storm surge heights alone do not have a great impact on increasing the future flood risk for the city.”

Sea level rise

However, sea level rise is likely to affect the size of future storm surges, the results suggest. Gardner says:

“The bad news is that when sea level rise is added into the picture, it becomes clear that overall flood heights will become drastically worse in New York City in coming years.”

Glossary

RCP4.5: The RCPs (Representative Concentration Pathways) are scenarios of future concentrations of greenhouse gases and other forcings. RCP4.5 is a “stabilisation scenario” where policies are put in place so atmospheric CO2 concentration levels off around the middle of the century, though temperatures do not stabilise before 2100. These policies include a shift to low-carbon energy technologies and the deployment of carbon capture and storage. In RCP4.5, atmospheric CO2 sits at 540ppm by 2100 – roughly 140ppm higher than now – equivalent to 630ppm once other forcings are included (in CO2e). By 2100, global temperatures are likely to rise by 2-3C above pre-industrial levels.

RCP4.5: The RCPs (Representative Concentration Pathways) are scenarios of future concentrations of greenhouse gases and other forcings. RCP4.5 is a “stabilisation scenario” where policies are put in place so atmospheric CO2 concentration levels… Read More

In addition, the researchers used existing scenarios that considered the potential impact of changes to the Antarctic ice sheet (AIS) (red, maroon).

The latest assessment report from the Intergovernmental Panel on Climate Change (IPCC) estimates the contribution of the AIS to sea level rise could be -8 to 15cm under RCP8.5 by 2100 (pdf).

Glossary

RCP8.5: The RCPs (Representative Concentration Pathways) are scenarios of future concentrations of greenhouse gases and other forcings. RCP8.5 is a scenario of “comparatively high greenhouse gas emissions“ brought about by rapid population growth, high energy demand, fossil fuel dominance and an absence of climate change policies. This “business as usual” scenario is the highest of the four RCPs and sees atmospheric CO2 rise to around 935ppm by 2100, equivalent to 1,370ppm once other forcings are included (in CO2e). The likely range of global temperatures by 2100 for RCP8.5 is 4.0-6.1C above pre-industrial levels.

RCP8.5: The RCPs (Representative Concentration Pathways) are scenarios of future concentrations of greenhouse gases and other forcings. RCP8.5 is a scenario of “comparatively high greenhouse gas emissions“ brought about by rapid population growth,… Read More

However, the authors of the new study note that recent research using “a coupled ice sheet and climate dynamics model that includes marine ice sheet instability, ice shelf hydrofracturing, and marine ice-cliff collapse mechanisms suggests that the AIS could contribute more than 1m by 2100, and more than 10m by 2300, under RCP8.5.”

Although there is “deep uncertainty” around the contributions of the Antarctic ice sheet to sea level rise, the authors write, “the potential for large contributions should not be neglected in risk assessments”.

Projected sea level rise in New York City from 2010 to 2300. Yellow shows projected sea level rise under an intermediate emissions scenario (RCP4.5), while orange shows projected sea level rise under a high emissions scenario (RCP8.5). Red and maroon show scenarios that also consider the likely effects of changes to the Antarctic ice sheet (AIS) Source: Garner et al. (2017)

The results suggest that, under the high emissions scenario, sea levels close to New York are likely to rise by 0.55-1.4m between 2010 and 2100. If the possible effects of Antarctic ice melt are considered, sea levels could rise by 0.88-2.5m by 2100.

The researchers combined their measurements of projected sea level rise and projected storm surge heights in order to estimate the total height of floods in New York in the coming decades.

The results show that flood heights in New York from 2080 to 2100 could be 1.4m above the average flood heights witnessed from 1970 to 2005, when an average is taken from all the scenarios of future sea level rise.

And serious floods, which exceed more than 2.25m in height, could dramatically increase in frequency over the coming decades, Garner explains:

“When rising sea-levels combine with storm surge heights, flooding becomes much worse over time. For example, a 2.25m flood height, which occurred on average once every 500 years before 1800 in our work, and occurred once every 25 years on average from 1970-2005 in our study, could occur once every five years by 2030-2045 according to our results.”

Such floods could pose a significant risk to human safety, she adds.

“A flood height of 2.25m is a significant enough flood to potentially inundate the first story of many buildings. Post-Sandy, some infrastructure and planning is almost certainly trying to account for future flooding situations, but a flood of this magnitude in New York would certainly still have significant impacts for many aspects of the city.”

Preparing the floodgates

The findings should prompt city planners to face up to the challenges posed by climate change, says Garner:

“Studies like this make it clear that adaptation measures are critical to protect lives and infrastructure in a changing climate. We can’t pretend that these kinds of risks aren’t growing in our changing climate, because studies such as this make it poignantly clear that they are.”

Also, looking as far out into the future as 2300 means the study relies on uncertain assumptions about factors such as future greenhouse gas emissions, he tells Carbon Brief:

“The paper assesses coastal flood risk over the next three centuries, but these risks depend hugely on scenarios as to how factors such as emissions and population size change. This makes me quite uncomfortable: the assumptions are huge and understated.”

It’s also worth noting that other nearby cities, such as Hoboken in New Jersey, are “every bit or more vulnerable” than New York City, Trenberth adds.